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1 A Comparison of Response Technologies for Offshore Oil Spills Exxon Valdez and BP Gulf of Mexico Oil Spills By Shuyu Chen Submitted to the Graduate Faculty of North Carolina State University in partial fulfillment of the requirements for the Degree of Master of Environmental Assessment Raleigh, North Carolina 2018 Approved by advisory committee: Dr. Waverly Kallestad, Committee Co-Chair Dr. Barry Goldfarb, Committee Co-Chair DEC 17, 2018

A Comparison of Response Technologies for Offshore Oil Spills

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1

A Comparison of Response Technologies for Offshore Oil Spills

Exxon Valdez and BP Gulf of Mexico Oil Spills

By

Shuyu Chen

Submitted to the Graduate Faculty of North Carolina State University

in partial fulfillment of the requirements for the Degree of

Master of Environmental Assessment

Raleigh, North Carolina

2018

Approved by advisory committee: Dr. Waverly Kallestad, Committee Co-Chair

Dr. Barry Goldfarb, Committee Co-Chair

DEC 17, 2018

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ACKNOWLEDGMENTS The author would like to thank Dr. Waverly Kallestad (NCSU) for her technical, kind, and unrelenting guidance; Dr. Barry Goldfarb (NSCU) for his technical guidance, organizational assistance, and prompt response during the development and completion of this project. In addition, the advisement and assistance from Dr. Linda Taylor and Sarah Slover in the successful completion of this degree is appreciated.

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ABSTRACT

The Exxon Valdez oil spill (EVOS) in Prince William Sound, Alaska in 1989 and the

BP Deepwater Horizon (DWH) oil well blow-out in the Gulf of Mexico in 2010 are

considered the two worst oil spills in North American history. The released oil caused

devastating impacts to the marine ecosystem. The nature of these two oil spills and

the spill locations were vastly different; therefore, their environmental impacts and

remediation technologies are also different. The purpose of this research is to conduct

a literature review to compare and contrast these two catastrophic oil spills and

determine which long-term remediation treatments (beside initial response approaches,

e.g., booms, control ignitions) were/are most effective and least invasive given the

different environments in which the oil spills occurred. After analyzing and

comparing the environmental conditions and remediation treatments of these two oil

spills, bioremediation, the acceleration of degradation processes through stimulation

of microorganisms, is considered most effective over the long term. Bioremediation is

a non-invasive and cost-effective process compared to the traditional physical oil

removal methods. However, a combination of approaches is often most effective for

response approaches and longer-term remediation strategies. Ultimately, the most

effective approach is to avoid oil spills.

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Table of Contents

ACKNOWLEDGMENTS .......................................................................................... 2

ABSTRACT .................................................................................................................. 3

TALBE OF CONTENTS ............................................................................................ 4

INTRODUCTION ....................................................................................................... 5

Composition and Toxicity of Petroleum Hydrocarbons .......................................... 5

Degradation Pathways.............................................................................................................10

Response and Remediation Approaches ............................................................... 10

DISCUSSION ............................................................................................................. 11

Comparison of Exxon Valdez Spill and BP Deepwater Horizon Spill ................. 11

Remediation Options ..............................................................................................................18

Biodegradation and Microbial Community.....................................................................21

Bioremediation.........................................................................................................21

Biostimulation............................................................................................................23

Bioaugmentation.......................................................................................................25

CONCLUSIONS ........................................................................................................ 28

REFERENCES ........................................................................................................... 29

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INTRODUCTION Every year, it is estimated that over 40 million gallons of crude oil are released into

the marine environment (Kvenvolden & Cooper, 2003). Nearly half of this is caused

by natural oil seepage, and the remainder is the result of human activities such as

petroleum extraction and transportation (Kvenvolden & Cooper, 2003). When oil is

released into water, it immediately undergoes a series of changes in both physical and

chemical properties. The changes include evaporation or volatilization, emulsification,

dissolution, and oxidation (abiotic: chemical, photo-degradation; and biotic:

microbial). This combination of degradation reactions is called the oil weathering

process (Fingas, 2012; Board, 2003).

When oil seepage occurs slowly, microbial communities are exposed to slow

diffusive hydrocarbon fluxes (Joye et al., 2010). In this manner, the microorganisms

indigenous to natural oil seeps are physiologically adapted to this environment and

use these hydrocarbons as their energy (carbon) source (Hazen et al., 2010). As a

result, ecosystems are generally capable of adapting to the natural oil seeps’ presence

and thus, of maintaining ecological balance. However, oil spills caused by human

activities typically rapidly release oil in quantities that overwhelm the threshold and

adaptation capabilities of the ecosystem (Eykelbosh, 2014). As such, damage may

occur at the various ecosystem levels including at the individual, population,

community and overall ecosystem levels. The problem becomes more complex when

the spatial, temporal scales and the inherent variability of the system are also

considered (Board et al., 2003).

Composition and Toxicity of Petroleum Hydrocarbons

Petroleum oil is a complex mixture of organic compounds including hydrocarbons,

nitrogen- and sulfur-containing molecules, and some heavy metals such as vanadium

(Saadoun, 2015). Petroleum hydrocarbons are comprised of a wide range of molecular

weights and structures that are divided into four classes (Fig1): 1) the saturates

(alkanes), 2) aromatics: monocyclic aromatics (BTEX) (benzene, toluene,

ethylbenzene and xylene) and Polycyclic aromatic hydrocarbons (PAHs) (e.g.,

naphthalene, anthracene and phenanthrene), 3) nonhydrocarbon, high-molecular-

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weight polycyclic organic substances that contain N, S and O atoms including

asphaltenes and waxes (phenols, fatty acids, ketones, esters, and porphyrins), and 4)

resins (pyridines, quinolines, carbazoles, sulfoxides, and amides) (Colwell et al., 1977;

Tissot & Welte,1984).

Figure 1. The four classes of petroleum hydrocarbons (Brown et al., 2017)

Generally, all oil components can exhibit both acute and chronic toxicity effects on

the marine ecosystem and marine organisms. The relative concentrations drive the

potential for adverse effects. When the oil components are floating on the ocean

surface as well as entrained in the water column (i.e., either present in the dissolved

aqueous phase and/or entrained with particulate material or dispersants), they are

acutely toxic because they are readily bioavailable to aquatic organisms. If the

weathering process is inhibited, oil can persist when buried in anoxic, nutrient-limited

sediments (Boufadel et al., 2010), this can lead to chronic biological exposures. As a

result, adverse effects on the reproductive systems of various organisms can result and

indirectly suppress the population recovery of exposed animals for decades. For

example, fish embryos exposed to weathered oil over the long-term could experience

deformities, reproductive mutations or even mortality (Teal & Howarth, 1984; Bodkin

et al., 2002; Culbertson et al., 2007; Esler &Iverson, 2010; Charles et al., 2011). A

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decadal database of herring biomass showed that adult herring are especially

vulnerable to damage from oil spills, in one instance this was observed as a

population decline over a 5-year period (Harwell & Gentile, 2006; Throne & Thomas,

2007).

The 1) Saturates (Alkanes) with the lowest molecular weights are volatile at low

environmental temperatures. They may display acute toxicity, but they evaporate so

quickly on the surface of the ocean that their impacts are generally small. However,

when released in deep water the saturates lead to greater toxicity because of their

water solubility, even though they biodegrade rapidly. The 2) mono-aromatics and

polycyclic aromatic hydrocarbons (PAHs) represent the most toxic fraction, and as

such possess the greatest potential for ecological and toxicological adverse effects.

The 3) nonhydrocarbon (asphaltenes) and 4) resins are resistant to biodegradation and

are very persistent, so they are more chronically toxic (IPIECA, 2015). Among these

four classes, the monocyclic and polycyclic aromatics are typically the most

toxicologically relevant.

Aromatics are comprised of mono- and poly-aromatic hydrocarbons. The mono-

aromatic hydrocarbons are collectively referred to as BTEX (benzene, toluene, ethyl-

benzene, and xylenes). BTEX comprise a significant percentage of petroleum pre-

cursor chemicals (Doherty & Otitoloju, 2016). They are used extensively in a number

of manufacturing processes, including the production of synthetic materials, fuel

additives, and consumer products (Wilbur & Bosch, 2004). About 90% of BTEX are

released into the atmosphere through the combustion of fossil fuels (Bolden et al.,

2015). BTEX have relatively high in water solubility, and they tend to evaporate into

the air from soil. Because they are relatively hydrophilic, they do not tend to sorb to

soil particles and can be transported long distances (Wilbur & Bosch, 2004). BTEX

compounds are listed as priority pollutants by the U.S. Environmental Protection

Agency (Fay et al., 2007). Prolonged exposure to BTEX compounds may have

adverse effects on both human health (e.g., damage the central nervous system

(ATSDR, 1993) as well as ecosystem functions (Khodaei et al., 2017). Some studies

indicate that benzene can cause acute leukemia, and ethylbenzene is carcinogenic in

organism tissues (Wilbur & Bosch, 2004).

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Figure 2. The molecular structure of the 16 polycyclic aromatic hydrocarbons (PAHs)

selected as priority pollutants by the U.S. Environmental Protection Agency (EPA).

Numbers are molecular weights (Henner et al., 1997).

Polycyclic aromatic hydrocarbons (PAHs) are a class of fused-ring multi-aromatic

ring compounds that are ubiquitous environmental pollutants caused by fossil fuel

combustion (Brooijmans et al., 2009). They are comprised of two or more fused

aromatic rings with a diverse range of branching types. Although aromatic molecules

are naturally occurring compounds (Dong et al., 2014) (Fig 2), they are also

environmental contaminants, which are somewhat resistant to environmental

degradation due to their hydrophobic nature (Gan & Ng, 2009). The PAHs found in

oil are also particularly resistant to microbial degradation, by the intrinsic stability of

the aromatic ring. PAHs are toxic and/or carcinogenic (depending on the specific

analyte) and persist in the oil-polluted environments long after the (linear) alkanes are

degraded. There are several hundreds of chemically related compounds, with various

structures and varied toxicity in PAHs (Abdel-Shafy & Mansour, 2016). The most

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common aromatic hydrocarbons with two rings are naphthalenes. The three-ring

compounds are anthracene and phenanthrenes (National Academies of Sciences,

Engineering, and Medicine, 2016). PAHs can cause carcinogenic and mutagenic

effects and are potent immune-suppressants (Armstrong et al., 2004) (Table 1). After

marine animals ingest PAHs, the enzymes in liver activate PAHs making them more

toxic as reactive metabolites. These aliphatic hydrocarbons in PAH metabolites are

highly oxidative and carcinogenetic because of their ability to bind to DNA and

proteins (Lin & Tjeerdema, 2010). PAHs containing up to six fused aromatic rings

are called “small” PAHs, and those containing more than six aromatic rings are called

“large” PAHs. Small PAHs are more predominant in the environment, such as

phenanthrene and anthracene (Armstrong et al., 2004).

No. Rings Log Kow Toxicity Reference

Naphthalenes 2 3.29 Acute toxic, Carcinogenic EPA, 1982

Anthracene 3 4.45 Not Carcinogenic

Hansch et al., 1995

Phenanthrenes 3 4.46

Not Carcinogenic

Hansch et al., 1995

Table 1. Selected chemical properties and example toxicities of 2- and 3- ring PAHs

These four classes of hydrocarbons are subject to different rates of microbial

biodegradation, due to the susceptibility of hydrocarbons to microbial attacks, driven

in large part by their chemical composition, structures, and physico-chemical

properties. In general, the biodegradability of the oil components generally decreases

in the following order: n-alkanes > branched-chain alkanes > branched alkenes > low-

molecular-weight n-alkyl aromatics > monoaromatics > cyclic alkanes > polycyclic

aromatic hydrocarbons (PAHs) ≫ asphaltenes (Van Hamme et al., 2003). Some high

molecular weight compounds, such as asphaltenes, may not be degraded at all,

depending on the surrounding environment and whether they are present in surficial

sediment or buried (Atlas & Bragg, 2009a). The persistence of petroleum

hydrocarbons in the environment is a critical factor for determining the magnitude of

adverse effects.

Degradation Pathways

There are two natural degradation pathways for oil spills, divided broadly into abiotic

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(chemical) and biotic (biological) degradation. Abiotic pathways, such as photo-

degradation, transform higher molecular weight alkanes and PAHs, especially larger

PAHs, rapidly by sunlight into more water-soluble oxygenated compounds or into

smaller degraded organic molecules (Yu, 2002). This is an extremely important initial

step in promoting bioavailability and further degradation of the resistant petroleum

compounds (Kings et al., 2014). Biotic degradation is facilitated by microbes, which

metabolize petroleum hydrocarbons as a food (i.e., carbon) source (Brooijmans et al.,

2009). Biodegradation is very effective in degrading small molecule petroleum

components, such as alkanes, alkenes, and small polycyclics. For high-molecular-

weight hydrocarbon classes, microorganisms produce extracellular enzymes and

biological surfactants (such as glycolipids, lipopeptides, lipoproteins or heteropoly‑

saccharides) to assist natural oil degradation (Ziervogel et al., 2012; Desai & Banat,

1997). Anaerobic biodegradation of petroleum components has frequently been

observed in nature (Widdel & Rabus, 2001). Anaerobic microbial processes are also

significant for degrading aromatic compounds such as BTEX compounds, by using

either nitrate or sulfate as an electron acceptor (Boopathy et al., 2012). The anaerobic

transformation of benzene and toluene under methanogenic conditions is similar to

fermentation, in which the substrate is partially oxidized and partially reduced,

yielding carbon dioxide and methane as end products (Mihelcic & Luthy, 1988). The

rate of biotic biodegradation depends mainly on the physiological capabilities of the

microorganisms and the hydrocarbon classes. In general, aerobic processes are faster

than anaerobic processes, and low-molecular-weight hydrocarbons are degraded more

quickly (Kleindienst et al., 2015). The rates of biodegradation also depend on the

physical state and concentration of the oil and environmental conditions, such as

temperature, oxygen level, nutrients (fertilizer), and the presence of biosurfactants,

(Brooijmans et al., 2009; Leahy & Colwell, 1990).

Response and Remediation Approaches

Traditional (i.e., historical) oil cleanup operations involve the use of toxic cleaning

agents or inappropriate methods that may cause more harm to the ecosystem than no

treatment. For example, the consequences of applying pressurized aqueous washing to

oily, rocky, intertidal communities contaminated by Exxon Valdez oil were tested.

Studies revealed that pressurized hot-water washing induced greater macro-algal and

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invertebrate mortality than the oiling itself (Mearns, 1996; Peterson, 2011). Therefore,

it is important to select response approaches and remediation strategies to treat oil

spills that are as environmentally safe and effective as possible with the ultimate goal

of eventually restoring ecosystem balance. The most common oil spill remediation

methods involve physical oil containment and skimming with floating booms, and

chemical or biological approaches such as applying chemical dispersants or biological

agents to enhance oil degradation (Fingas, 2012). The DWH spill, which was the

largest emergency response to a marine oil spill in history included dispersant

application, controlled burn, skimming, siphoning from the wellhead, containment

booms, shoreline scavenging/berms, and beach sand mixing to mitigate the spill’s

impact.

Biodegradation of petroleum hydrocarbons by natural populations of microorganisms

represents one of the primary mechanisms to eliminate oil spill contamination from

the environment (Das & Chandran, 2011). The rates of biodegradation of oil spills are

dependent on both environmental and biological factors. In addition, applying

biodegradable dispersants and surfactants instead of toxic chemical-based solvents

helps to accelerate the biodegradation process, and hence, reduce the environmental

impact of the oil spill (Nyankson et al., 2016).

DISCUSSION

As the introduction has demonstrated, while generalizations can be made regarding

petroleum hydrocarbon behavior in the environment following an oil spill, the

location of the actual spill can better inform appropriate response approaches, which

remediation technologies are most effective, and the potential for adverse effects.

Factors that influence fate and transport, as well as effects of spilled oil are discussed

below. Comparisons are drawn between the high latitude Exxon Valdez oil spill in

Prince William Sound, Alaska (1989) and the low latitude BP Deepwater Horizon oil

well blowout in the Gulf of Mexico (2010) (Table 2).

Table 2. Comparison of Exxon Valdez Spills, and BP Deepwater Horizon Spills

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Exxon Valdez (EVOS) BP Deepwater Horizon (DWH) 1. Location Prince William

Sound, Alaska (1989) Gulf of Mexico (2010)

2. Latitude 60° 49' 59.99" N (GeoHack - Exxon Valdez oil spill, n.d.)

28° 44' 11.99" N (GeoHack - Deepwater Horizon oil spill, n.d.)

3. Avg. Water Temperature

0-12 °C 20-27°C

4. Nutrients Sufficient in open water (Atlas & Bragg, 2009a), but deficient on rocky beaches (Schmidt, 2012).

Deficient (Atlas & Hazen, 2011). A large bloom of carbon-metabolizing microbes due to oil spills could deplete the surrounding nutrients (American Academy of Microbiolog, 2011).

5. Marine Environment

Vulnerable and pristine (Riedel, 2014). More enclosed and shallower than open ocean. Sub-Arctic region. Latitude just south of the arctic circle.

Robust system. Open ocean. Responds rapidly to the influx of oil, because indigenous microbiota are adapted to natural oil seeps in marine environment (National Research Council, 1985). Subtropical region. Latitude just north of the equator.

6.Oil Type and Degradation Speed

North Slope Heavy Crude Oil (API gravity 29.6) (Atlas & Hazen, 2011). Contained heavy, polar compounds such as resins, hopanes, and asphaltenes. Slow biodegradation rates (Atlas & Hazen, 2011).

Light Louisiana Crude Oil, and methane gas (CH4) (API gravity 35.2) (Atlas & Hazen, 2011). Lower molecular weight hydrocarbons are more biodegradable initially than heavy crude oil, which also biodegrades more rapidly than heavy crude oil (Atlas & Hazen, 2011).

7. Spill Volume 11 million gallons. Enclosed and shallower (Wolfe et al., 1994).

206 million gallons estimated by the National Incident Command’s Flow Rate Technical Group. Deeper and open ocean (Atlas & Hazen, 2011; Nyankson et al., 2006).

8. Spill Position in Water Column

Discharged as a surface spill (Atlas & Hazen, 2011).

Discharged at the wellhead in 1500 m water. As oil became weathered during ascent, color appeared reddish –brown and was less cohesive than crude oil when reaching the surface (Atlas & Hazen, 2011).

9. Spill Location

On Bligh Reef near island shorelines (Skinner & Reilly, 1989).

77 km offshore US southeast coastal states (Atlas & Hazen, 2011)

10. Spill Types The traditional shore- Novel, deep-ocean persistence of

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bound surface spill characterized by buoyant oil, fouling and killing organisms at the sea surface and eventually grounding on and damaging sensitive shoreline habitats (Peterson et al., 2012).

intrusions of finely dispersed oil, gas, and dispersants at 1500 m water depth with high pressure (Peterson et al., 2012). Impacted deep-sea, marshes and sandy beach shorelines with fine droplets of low concentration oil. (Atlas & Hazen, 2011).

11. Degradation Speed

It was estimated that there had been a 22% per year decline from 1991 to 2001 in the amount of oil remaining on the shore (Short et al., 2004).

Unbranched chain hydrocarbons can be degraded quickly in a matter of days or weeks. (American Academy of Microbiology, 2011).

12. Degradation Results

By 2003, more than 80% of alkanes are depleted, and more than 70% of PAHs are lost (Atlas& Bragg 2009a).

By August 2010, 78% of the oil is disposed off by either human intervention (direct recovery, in situ, burning, skimming, and dispersal) or natural processes (naturally dispersed, evaporated, and dissolved) (Ramseur, 2010), whereas the fate of the remaining 22% of the oil spill was uncertain.

13. Initial Response

Not applicable due to storms (Council, 2013).

Direct recovery from the wellhead, Control burning, skimming (Lubchenco et al., 2010)

14. Cleanup Strategies

Bioremediation and physical removal methods such as water washing were used extensively. Applied fertilizers containing Nitrogen. Nutrients increased the degradation process (Atlas & Hazen, 2011).

Photo-degradation significant (Nicodem et al., 1997)

Microbes played a major mitigating role. Aerial and subsurface dispersants used extensively. Physical methods such as booming, skimming, and controlled burns were used to mitigate spill’s impact. (Atlas & Hazen, 2011).

15.Role of Photo-degradation

Less important (Amon and Meon, 2004).

Very important (Nicodem et al., 1997)

16. Use of Dispersant

Only 4000 gallons of dispersants were used Lack of waves and regulation concerns of

Aerial and subsurface dispersant used immediately and extensively (Atlas & Hazen, 2011).

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Petroleum degradation processes are very complex. There are various factors that

determine the rates of biodegradation, including: 1) Physical state of the oil spill (i.e.,

the classes of petroleum hydrocarbons and their behavior in the marine environment;

2) the location of the spill and the ambient chemical and physical oceanographic

properties of those locations (i.e. Artic Sea [high latitude] and the Gulf of Mexico

[low latitude], temperature, dissolved oxygen concentrations, nutrients/nutrient

limitations); 3) remediation options (i.e., use of dispersants and biosurfactants) and 4)

the biological composition, especially the presence and composition of the microbial

communities of the affected environments (Saadoun, 2015).

The greatest difference between DWH oil spill and EVOS was more than an order of

toxicity (EPA, 2016) 2.1 million gallons of dispersant applied. (Nyankson et al., 2006)

17. Limitation Factor

Temperature and nutrients. (Boopathy et al., 2012; Boufadel et al., 2010).

Nutrients and oxygen level (Nicodem et al., 1997)

18. The Fate of Oil Remnants

Still under study almost 25 years after the spill (Atlas & Hazen, 2011)

Roughly 45% to 76% of the discharged hydrocarbons were constrained within five years (Joye, 2015)

19. Type of Exposure (Risk Assessment Model)

Long term, chronic persistence toxic oil components, such as PAHs, may remain buried in sediment, released by bioturbation or human activities. (McGenity et al., 2012)

Selective, largely short-term, acute toxicity (McGenity et al., 2012). (Perhaps with exceptions to near-shore wetland areas).

20. Microbe Community Adaption

Adapted to Cold Temperature. (American Academy of Microbiology, 2011)

At a depth of over 1500 meters, the temperature is low, and pressure is high. The microbial species are adapted to these extreme conditions. (American Academy of Microbiology, 2011)

21. Focus on Biodegradation

Shorelines, oil concentrate at the surface of the water

A unique deep-water cloud of dispersed oil

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magnitude in a total volume of oil spills (DWH 205.8 million gallons versus EVOS

11 million gallons). DWH spill also released unprecedented amounts of methane gas

into the water column (CH4) (Fernández‐Carrera et al., 2016). The rapid natural

degradation of oil in the DWH spill is due to a number of factors, such as the type of

crude oil, offshore, jetting of the oil in to the deep-sea, rapid dissolution, and

microbial adaption (Atlas & Hazen, 2011). The EVOS occurred near shore and

occurred as a surface slick, while the DWH blowout was a leak from a well 1500 m

below the ocean surface, which forms both a deep-sea “cloud” and a surface water

slick, more than 80 km from the nearest shore (Atlas & Hazen, 2011). The

environments impacted were also very different in terms of climate, weather, and

ecosystems, EVOS occurred in a sub-Arctic region and the DHW spill occurred in a

subtropical region. The Gulf of Mexico has numerous natural oil seeps, greater than

any other marine area in North America, contributing more than 400,000 barrels of oil

a year to the Gulf of Mexico (Board et al., 2003). The microbiota are better adapted to

oil because of natural seeps and offshore drilling activities and as such, the

biodegradation process is very rapid. This is in contrast to the relatively pristine

conditions of Prince William Sound which is much more enclosed and shallower than

the open ocean environment in the Gulf of Mexico (Atlas & Hazen, 2011).

Oil spilled in water tends to spread and form a slick (Berridge et al., 1968). The larger

and thicker the slick, the less surface area for microbes; therefore, the degradation is

slower. A fine dispersion of droplets of oils in the water column in the form of oil-in-

water state, called emulsions, increases the surface area of the oil. Therefore, this

form is more prone to microbial attack. On the contrary, tarballs, which are large

aggregates of solidified crude oil, inhibit biodegradation, due to low surface-to-

volume ratios of oil to water. The lighter the oil, the faster this diffusion, making the

petroleum more available to the microbes (American Academy of Microbiology,

2011). In addition, weathering factors such as precipitation and wave action highly

influence the rate of degradation (Davis & Gibbs, 1975). The type of oil released from

EVOS was North Slope Heavy Crude Oil (API gravity 29.6) (Atlas & Hazen, 2011).

It contains high-molecular-weight, polar compounds such as resins, hopanes, and

asphaltenes that have nominal biodegradation rates (Atlas & Hazen, 2011). In contrast,

the type of oil released from DWH was Light Louisiana Crude Oil; This oil contains

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many unbranched simpler lower molecular weight hydrocarbons and methane gas

(CH4) (API gravity of 35.2) (Atlas & Hazen, 2011). Therefore, the light Louisiana

crude oil released from DWH spill biodegraded more readily than heavy crude oil

from EVOS.

Among physical factors, temperature plays the most important role in biodegradation

of hydrocarbons by affecting the oil’s physical properties, the chemical composition

of the pollutants, solubility of hydrocarbons, as well as affecting the physiology and

diversity of the microbial flora and its activities (Atlas, 1981; Das & Chandran, 2011;

Foght et al., 1996). Petroleum hydrocarbons can be biodegraded at temperatures

below 0 ° to more than 80 °Celsius (Das & Chandran, 2011). The rate of

biodegradation decreases with decreasing temperature. At low temperature, the

viscosity of the oil increases and the volatilization of toxic short-chain alkanes is

reduced, therefore slowing the biodegradation. Higher temperature increases the rate

of enzymatic activities of the microbial community, thus increasing the

biodegradation processes (Atlas & Bartha, 1972; Gibbs, 1975). The highest

degradation rates occur in a range of 15–20°C in marine environments (Cooney,

1984). This indicates that relative to temperature degradation, the waters of the Gulf

of Mexico would be more conducive to hydrocarbon degradation than the waters of

Prince William Sound (i.e., 20-27°C vs. 0-12°C, respectively).

Generally, oil creates a slick that covers the surface of the water. This physical

coating prevents seawater from absorbing oxygen from the atmosphere. In open

waters, the oil spill exhibits oxygen-depleting effects from the surface waters all the

way to the seafloor (Biello, 2010). However, conditions of oxygen limitation

generally do not exist in the upper levels of the water column in marine environments

(Floodgate, 1984). Nevertheless, the aquatic sediments are usually anoxic (Hambrick

et al.,1980). Moreover, the rich fertilizer carried into the Gulf of Mexico estuaries

region from inland farms and runoff prompts blooms of algae, phytoplankton, and

other microscopic plants. Their decomposition depletes the oxygen in seawater,

creating a vast dead zone that is lethal to sea life (i.e., anthropogenic eutrophication).

An oil spill could exacerbate the situation (Biello, 2010). On the contrary,

the EVOS did not create such dead zones near shore. The dissolved oxygen levels

were lower than optimal values for oil biodegradation (Boufadel et al., 2010), but

17

currents promoting air- water column mixing there minimized the damage to sea life

(Atlas& Bragg, 2009b).

Nutrients are very important factors for successful biodegradation of petroleum

hydrocarbon pollutants. Some nutrients can act as limiting factors because

microorganisms require elements in addition to carbon for growth. The concentrations

of inorganic nitrates (NO3), phosphates (PO43-), and iron (Fe) in the marine

environment can limit rates of oil biodegradation (Atlas, 2011). The marine

environment was found to contain fewer nutrients than freshwater because seawater

had lower levels of nitrogen and phosphorous (Floodgate, 1984). Consequently, it is

necessary to add nutrients in order to facilitate biodegradation (Choi et al., 2002).

Studies have shown that fertilizers are most effective in the first weeks after the spill

and speed up the natural biodegradation process (Pelletier et al., 2004)). However,

fertilizers may impose a negative impact on certain hydrocarbon biodegradation

processes. For example, PAH biodegradation values were higher when nutrients were

not added (Vinas et al., 2005). The biodegradation activity can also be inhibited if

there is excessive nutrient concentration (Chaillan et al., 2006). The use of fertilizers

under severe weather conditions in artic regions seems to be beneficial, as low

temperatures tend to slow down bacterial growth. In EVOS, even though there were

sufficient concentrations of nutrients and oxygen in the open waters to support

biodegradation processes (Atlas & Bragg, 2009b), the nutrients were deficient on the

rocky beaches where the majority of spilled oil washed. Consequently, the limited

water flow limited biodegradation rates (Boufadel et al., 2010, Li & Boufadel, 2010).

The offshore waters of the Gulf of Mexico are oligotrophic in nature. Bacterial

activities in the DWH oil spill show enhanced microbial respiration, but signs of

phosphate stress indicated this nutrient was a factor limiting the rate of biodegradation

(Edwards et al., 2011). This is due to the sudden input of carbon (oil spills) to the

Gulf of Mexico causing a large bloom of carbon-metabolizing microbes, and the

subsequent nutrient depletion limiting microbial activity.

Photo-degradation

Particularly in the ocean at low latitudes, where seawater receives a high solar flux

but is nutrient depleted, the microbial activities are limited, making photo-degradation

processes pervasive (Ehrhardt et al., 1992). For example, photo-degradation was

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extensively observed in the Deepwater Horizon oil spill. In addition, for low

molecular weight volatile oil components, evaporation from seawater followed by

photooxidation in the air was also a key process (Cox et al., 1981; Mantoura et al.,

1982; Nicodem et al., 1997). This was a less important mechanism for EVOS in

Prince William Sound, AK, because low solar angles minimized the solar radiation

availability to aquatic photo-degradation processes (Amon and Meon, 2004). Photo-

degradation processes may also interfere with biodegradation, because photo-

degraded PAHs may produce a toxic substance that is harmful to microorganisms

(Kings et al., 2014; Bertilsson & Widenfalk, 2002). Thus, photo-enhanced toxicity

could contribute to the toxicity of crude oil in the field.

Remediation Options

Dispersants

According to the “Oil Spill Response Field Manual” by ExxonMobil (ExxonMobil,

2014), the first response approach to an oil spill is oil containment and skimming. It

is the most effective method if the spill is accessible within a few hours from onset.

However, in the EVOS and DWH spills, oil containment and skimming were not

applied because a storm with 80 km/h winds hit Prince William Sound within two

days of the initial spill resulting in an area too large to contain with floating booms

(Atlas & Hazen, 2011). Moreover, the DWH spill occurred at the wellhead in 1500m

water depth, so this method was also ineffective. Thus, practical approaches to oil

spill response containment strategies must be considered; booming and skimming

may not always be applicable. Applying both dispersants and other biological agents

to enhance oil degradation were the two major strategies implemented in these two

spills. Artificial dispersants can break up oil slicks and emulsify oil in water, leading

to the formation of small droplets and make the oil potentially available for

biodegradation (Kleindienst et al., 2015). Chemical dispersants also dissolve oil in

water, and reduce oil accumulation at the water surface. Furthermore, chemical

dispersants potentially stimulate microbial biodegradation of oil by increasing the

surface area of oil. As a result, they make the oil more available to marine

communities. However, some dispersant formulations can themselves pose impacts

on the marine organisms and environment or inhibit microbial processes.

Nevertheless, according to the US National Research Council, the acute lethal toxicity

19

of chemically dispersed oil are primarily the result of alkenes and dissolved aromatic

and aliphatic fractions of the oil (Board & National Research Council, 1989). For

example, most dispersed oil remains in the water column, and this fraction

subsequently threatens pelagic and benthic organisms (NRC, 2005).

The USEPA has conducted acute, short-term toxicity tests on dispersants, and

confirmed low to moderate toxicity (Hemmer et al., 2011). Analyses of tests

conducted on a variety of aquatic species showed that compared with fish, crustaceans

are more sensitive to oil dispersant exposure (George-Ares & Clark, 2000).

Ramachandran et al., (2004) suggest that the use of oil dispersants increases the

exposure and uptake of PAHs by fish. The impact of PAH toxicity on sensitive life

stages, such as eggs and larvae, is enhanced by chemical dispersion (McConville et

al., 2018; Negri et al., 2018). On the contrary, Fingas et al., (1991) suggested that

dispersants possess low toxicity and do not increase the toxicity of the dispersed oil,

because they are present in the water column at very low concentrations (Fingas et al.,

1995). Toxicity is dependent on both concentration and exposure time. Wells (1984)

reported that dispersants would need to be present in the water column at hundreds of

parts per million for over several days to exert either lethal or sub-lethal toxicities.

Wells (1984) conducted extensive laboratory studies. In addition, the effectiveness of

dispersants has been shown to be extremely variable depending on the specific oil

type. In general, one-part dispersant will disperse about 20–30 parts of oil. When

dispersing the light oil with optimum sea energy, it could reach over 100 parts of oil

per part of dispersant (Mackay, 1995). Heavy (i.e., low API gravity) and weathered

oils are more resistant to dispersion and may require a higher ratio of dispersant to oil.

Highly viscous, non-spreading oils and waxy oils may resist chemical dispersion

altogether (Lessard & DeMarco, 2000).

During the early phases of an oil spill, applying dispersants may prevent or reduce

impacts on coastal habitats, wildlife, and property. However, dispersant use is not

universally recommended for all spills and habitats due to limitations in the rate or

capacity for immediate mixing and dilution. So, the necessity of oil dispersant use is

sometimes questioned (American Society for Testing and Materials, 1997).

In the case of the DWH, the application of 1.07 million gallons of dispersants onto the

sea surface and injection of 0.77 million gallons of dispersant directed toward the

20

wellhead was controversial. Because this blowout occurred in deep offshore water

(1500 m), the highly turbulent discharge of hot, pressurized oil and gas could have

produced a variety of dispersed phases, including small oil droplets, gas bubbles, oil-

gas emulsions, and gas hydrates (Federal interagency solutions group, 2010). This

turbulent mixing induced by pressurized oil and gas into cold seawater was sufficient

to induce massive dispersion of oil into fine droplets while creating emulsions of oil,

gas, water, and gas hydrates. (Johansen et al. 2003; Federal Interagency Solutions

Group, 2010). Moreover, dispersants applied to weathered oil at the sea surface

during windy days had sufficient surface mixing to be effective; whereas, on calm

days, the dispersants were largely ineffective (Fingas, 2001). In EVOS, dispersants

were only performed in a trial application stage. Only about 4,000 gallons of

dispersant were applied, and the effects were diminished due to lack of wave action to

mix the dispersant with the oil in water (EPA, 2016). Weather affects dispersant

application and effectiveness in three ways: 1) the amount of dispersant that contacts

oil is highly wind-dependent, 2) the amount of oil dispersed on the water surface is

dependent on ocean turbulence and other energy, and 3) the amount of oil remaining

in the water column is also dependent on the same energy. The higher the wind, the

less dispersant will be applied to the oil from an aerial platform, but the greater the

mixing with the water column. The greater the sea energy, the more oil will be

dispersed downwards and the more it will stay dispersed (Fingas & Ka’aihue, 2004).

During the DWH spill, over 2.1 million gallons of dispersant were applied to

minimize the impact of this disaster (Nyankson et al., 2006). The use of dispersants

resulted in a significant reduction of oil reaching the shore, which reduced the

immediate threat to beaches and salt marshes. The effects of dispersants on the

biodegradation in the deep plumes are unknown (American Academy of

Microbiology, 2011). However, environmental and toxicity issues arose over the

usage of dispersant. After the DWH spill, various studies have been conducted to

research various remediation strategies. It has been recently discovered that some

environmental and biodegradable dispersants can replace the chemical dispersants in

order to reduce toxicity. Nyankson et al., (2006) examined the ability of dispersants

formulated with hydroxylated soybean lecithin solubilized in water to disperse crude

oil. The de-oiled soybean lecithin was hydroxylated and solubilized in water to

procedure the dispersant. The U.S. EPA’s test showed that the hydroxylated soybean

21

lecithin processed near complete dispersion effectiveness: (1) reducing the rigidity of

the fatty acid chain, (2) increasing interaction between the surfactant and aqueous film

at the interface, and (3) increasing the hydrophilicity of soybean lecithin. The findings

from this study suggest that a dispersant formulated from hydroxylated soybean

lecithin has the potential of replacing the traditional chemical dispersants in oil spill

remediation (Nyankson et al., 2015). However, this approach has yet to be tested

outside of the laboratory.

Biodegradation and Microbial Community

Bioremediation

Because the traditional oil cleanup operations include inappropriate methods that can

cause more harm to the ecosystem, bioremediation could play an important role in

restoration with minimum impact on the ecosystem. The process of bioremediation

involves using microorganisms to detoxify or remove pollutants through diverse

metabolic reactions. This is an evolving method to remove and degrade petroleum

pollution in the marine environment (Medina‐Bellver et al., 2005). This

bioremediation technology is considered to be noninvasive and relatively cost-

effective (April et al., 1999). It can effectively remove environmental contaminants,

contrary to physical and chemical methods, which usually cause dispersion of the oils,

are not effective in contaminant removal, and are very expensive (Khan et al., 2004).

Bioremediation of contaminated sites depends on the metabolic capacity of

indigenous microorganisms as well as environmental conditions (Yu et al., 2005).

There are the two main approaches to oil spill bioremediation: (1) biostimulation, in

which the growth of indigenous oil degraders is stimulated by the addition of nutrients

or other growth-limiting cosubstrates. (2) bioaugmentation, in which known oil-

degrading bacteria are added to supplement the existing microbial population (Das &

Chandran, 2011). One of the cleanup strategies employed in EVOS involved the

application of nutrients in the form of fertilizer to increase oil biodegradation rate

(biostimulation). Because bioremediation was used extensively in the EVOS, it has

become one of the primary mechanisms to clean up oil spills due to its effectiveness

and lower cost than other remediation technologies (Leahy & Colwell, 1990).

Bioremediation functions basically via biodegradation pathways, which can result in

22

the complete mineralization of organic contaminants into carbon dioxide, water,

inorganic compounds, and cell proteins or transformation of complex organic

contaminants to other simpler organic compounds by biological agents including

microorganisms.

Microbes have used oil as their source of energy for hundreds of millions of years

(American Academy of Microbiology, 2011). Because microbes can biodegrade up to

90% of light crude oil (American Academy of Microbiology, 2011), microbial

degradation is the major and ultimate natural mechanism that can clean up oil spills

(Atlas, 1984). No single microbe can break down all petroleum compounds, but the

combining action of the community can degrade almost all of the petroleum

components. Hydrocarbons in the environment are biodegraded primarily by bacteria,

yeast, and fungi (Das & Chandran, 2011). Several bacteria are even known for

feeding exclusively on hydrocarbons (Yakimov et al., 2007). Floodgate (2004) listed

25 genera of hydrocarbon degrading bacteria and 25 genera of hydrocarbon degrading

fungi, which were isolated from the marine environment. The genome of the obligate

hydrocarbon degrading bacterium Alcanivorax borkumensis has recently drawn the

interest of some researchers. It blooms in oil spill contaminated areas and can

constitute up to 80% of the bacterial population (Schneiker et al., 2006). The features

of its genome reveal how this bacterium grows efficiently on alkanes. As

hydrocarbons are poorly soluble in water, this bacterium encodes extensive

exopolysaccharide production, and it can attach to the oil‐water interface

(Brooijmans et al., 2009). In addition, cytochrome P450 (CYP450) alkane

hydroxylases constitute a super family of ubiquitous heme-thiolate monooxygenases,

which play an important role in the microbial degradation of oil (Van Beilen &

Funhoff, 1997). Depending on the chain length, enzyme systems are required to

introduce oxygen in the substrate to initiate biodegradation. CYP450 enzyme systems

were found to be involved in biodegradation of petroleum hydrocarbons. Such

CYP450’s are commonly found in higher eukaryotes in general but only in a few

species of microorganisms (Zimmer et al., 1996). CYP450 forms are also found in

several yeast species that use n-alkanes and other aliphatic hydrocarbons as a sole

source of carbon (Scheller et al., 1998).

Microbes can biodegrade up to 90% of light crude oil by volume but are not

23

significantly effective in degrading high-molecular-weight compounds such as

Asphaltenes and PAHs (American Academy of Microbiology, 2011). Some bacteria

can effectively break down PAHs, which involves whole communities of both

bacteria and eukaryotes (Brooijmans et al., 2009). Cycloclasticus (Piscirickettsiaceae)

is one of the important PAH-degrading bacteria (Dyksterhouse et al., 1995). It was

observed in one experiment that its growth pattern increased with PAH

biodegradation processes (Campeão et al., 2017). Even though bacteria can convert

PAHs completely to biomass, CO2, and H2O, they usually need the initial insertion of

O2 via dioxygenase enzymes (Atlas, 2011). Moisture content and aeration were

determined to be the key factors associated with PAH bioremediation (Vinas et al.,

2005). For instance, the PAHs from EVOS has persisted on several beaches in Prince

William Sound (PWS) for more than 20 years after the contamination. The current

degradation rate of the total PAH (TPAH) is estimated at 1% per year. Low oxygen

concentrations were the major factor causing this oil persistence. One bioremediation

method is by injecting of hydrogen peroxide and nutrients deep into four beaches in

Prince William Sound in the summers of 2011 and 2012. As a result, the TPAH

biodegradation rate was between 13% and 70% during this time. The results also

showed high efficiency in the delivery of oxygen and nutrients to the contaminated

areas of the beach. This method is especially effective in higher latitudes regions

(Boufadel et al., 2016). On the contrary, the PAHs at the Gulf of Mexico deplete

rapidly naturally in the open ocean, substantially due to photodegradation (King et al.,

2014). PAHs in the oil residues would also have undergone considerable weathering

such as volatilization and dissolution when transiting from the wellhead to the

shoreline (Yin et al., 2015). Nevertheless, preliminary findings show that PAHs in

the Light Louisiana Crude oil were rapidly depleted in the Gulf of Mexico

environment (Brown et al., 2011). One study showed that by 2012, 97.0% of the

TPAH fraction had already been lost (Atlas et al., 2015).

Biostimulation

Biostimulation involves the identification and adjustment of factors that may affect

the indigenous microorganism’s biodegradation rate of the contaminants of the

affected site (Swannell et al. 1996). These factors include type and concentration of

nutrients, physical and environmental parameters, chemical composition, physical

24

state and concentration of the crude oil or hydrocarbons; along with the temperature,

oxygen availability, salinity, pressure, water activity, and pH on the site (Leahy and

Colwell 1990). Petroleum hydrocarbons are a substantial carbon source for the

indigenous microorganism, whereas, the nitrogen and phosphorous nutrients, as

previously mentioned are commonly limiting. Thus, biostimulation accelerates the

biodegradation rate when adding these nutrients into the contaminants (Nikolopoulou

and Kalogerakis 2009; Prince 1997). Biostimulation technologies for beach cleanup is

the most effective (OTA , 1991). During the EVOS, biostimulation using fertilizers

containing N nutrients was the major strategy (Atlas & Hazen, 2011). Soon after the

incident, both the EPA and Exxon quickly conducted laboratory and field tests and

confirmed that the addition of fertilizer would enhance the rate of oil biodegradation

by the indigenous hydrocarbon-degrading microorganisms (Bragg et al., 1992;

Pritchard & Costa, 1991). As a result, rates of biodegradation in bioremediation

doubled (OTA, 1991). The rate of oil degradation was a function of the ratio of

Nitrogen/biodegradable oil and time. In addition, O2 dissolved in water was not a rate-

limiting factor (Atlas & Hazen, 2011). In all, 48,600 kg of Nitrogen in fertilizers were

applied from 1989 to 1991. This represents the largest use of bioremediation in

history (Zhu et al., 2001). A survey in 1992 found that most of the oil had been

removed from shorelines and on June 12, 1992, the U.S. Coast Guard and the State of

Alaska officially declared the cleanup concluded (though residual oil remained)

(Atlas & Hazen, 2011). However, this strategy wasn’t widely applied in the DWH

spills, located in a vast of open ocean, because it is very expensive and difficult to

keep the nutrient concentrations at levels that accelerate the speed of biodegradation

(Atlas & Hazen, 2011).

Moreover, biosurfactants can speed up the biodegradation process. Biosurfactants are

a heterogeneous group of surface-active chemical compounds produced by a wide

variety of microorganisms, such as yeast, bacteria, and fungi (Muthusamy et al., 2008;

Mahmound et al., 2008). Biosurfactants are amphiphilic compounds that attract both

lipids and water and reduce the surface tension between the two substances.

Biosurfactants emulsify alkanes and increase the oil‐water surface area (Brooijmans

et al., 2009). Therefore, it enhances solubilization and removal of contaminants

(Brusseau et al., 1995; Bai et al., 1997). Biodegradation is also enhanced by

25

biosurfactants due to increased bioavailability of pollutants because biosurfactants

facilitate the breakdown and dispersal of lipid molecules into smaller droplets (Barkay

et al., 1999). The microdroplets encapsulated in the hydrophobic microbial cell

surface are taken inside and degraded (Das & Chandran, 2011). Gross (2010)

proposed introducing biosurfactants in sufficient quantity to assist these organisms in

quickly converting the oil from the Deep Horizon spill. Currently, the major market

for biosurfactants is for oil spill cleanup, the removal of oil residue from storage tanks,

microbial-enhanced oil recovery, and the bioremediation of soil and water (Sobrinho

et al., 2013).

Bioaugmentation

More recently, scientists have been looking for new methods that are efficient and

environmentally safe to advance bioremediation. Bioaugmentation is another process

that enhances bioremediation. Bioaugmentation is the supplementation of highly

concentrated and specialized microbe populations (single strains or consortia) to the

contaminants (Leahy and Colwell 1990; Gentry et al. 2004). There are two categories;

1) introduction of special assemblages of naturally occurring oil-degrading

microorganisms (seeding) (Atlas, 1995), and 2) introduction of genetically engineered

microorganisms (GEMs) with special oil-degrading properties (Urgun-Demirtas et al.,

2006). In the first seeding method, these microorganisms can be cultivated in the

laboratory and then inoculated into the environment. As they are the indigenous

species in the environment, these microorganisms are adapted to the native

environment of the contaminated site compared with the non-indigenous groups

(Orcutt et al., 2010, Thavasi et al., 2011). It was reported that bioaugmentation,

tested in the laboratory, was a good strategy to accelerate the degradation of

components like n-alkanes, branched alkanes, and PAHs during the first five days

after contamination. After the early stage of the oil spill, the rate of biodegradation

slows down (McKew et al., 2007). This technique is most applied in the following

situations when the environment (1) does not have sufficient microbial cells present

or (2) the native population does not possess the metabolic routes necessary to

metabolize the contaminants of concern (Tyagi et al., 2011). By adding cultured

microorganism strains into the subsurface, it may increase the speed of degradation of

a contaminant (Herrero & Stuckey, 2015). However, in field tests, adding seed

26

cultures has proven less promising for treating oil spills than adding fertilizers and

ensuring adequate aeration because the widely distributed hydrocarbon degrading

bacteria and fungi naturally exist in the marine environment (Atlas, 1995). In addition,

applications for genetically engineered microorganisms (GEMs) have received

attention for improving degradation under laboratory conditions (Urgun-Demirtas et

al., 2006). The genetically engineered bacteria show higher degradative capacity than

non-genetrically engineered microorganisms. From a pratical perspective, using a

mixed bacterial consortium culture rather than a single-strain culture for the

bioremediation is more adavantaeous as it is more robust and diverserfied (Rahman et

al. 2002). There have been serveral successful laboratory experiments on GEM

bateria that resulted in major degradation of hydrobarbons, and the degradation rate

was significatly increased (Tyagi et al., 2011). However, due to the ecological and

environmental concerns and current regulatory constraints, the testing of GEM in the

field is still prohibited (Garbisu & Alkorta, 1999). Even though the field test of the

seeding technology is not as promising, there have been some successful cases. For

example, Rghavan & Vivekanandan (1999) reported that the application of natural

seeding bacteria to the oil spill area resulted not only in rapid multiplication of

bacteria but also accelerated the disappearance of the hydrocarbons. The combination

of microbiological and ecological knowledge, biochemical mechanisms, and field

engineering designs are essential elements for successful in-situ bioaugmentation

(American Academy of Microbiology, 2011).

The DWH oil spill provides a unique opportunity for scientists to understand the

significant roles that microbes play in the recovery process at oil-contaminated

environments. Different microbiological methods were applied to investigate the

changes and responses of bacterial communities after the spill (Zhang et al.,

2018). As of 2001, over 200 species of microbes (bacteria and fungi) that degrade

hydrocarbons had been discovered in oil (Zhu et al., EPA, 2001). Among these

species, some indigenous bacterial communities in different habitats (seawater, deep-

sea sediment, marshes, and beach sands) responded rapidly to the spilled oil and some

bacterial groups might play significant roles in reducing this type of environmental

contamination (Zhang et al., 2018). A class of bacteria called hydrocarbonoclastic

bacteria (HCB) have been the most active, globally, at degrading hydrocarbons in

27

marine environments (McKew et al., 2007). Recently, scientists have successfully

applied DNA synthesis and genome construction on marine bacteria that can break

down the different types of hydrocarbon chemicals in oil, including PAHs. For

example, Oceanospirillales, degraded alkanes in the Deepwater oil plume, whereas

Rhodospiralles was responsible for degrading PAHs (Hu et al., 2017). The

combination of stable isotope probing (SIP) and metagenomics techniques allowed

for the reconstruction of hydrocarbon degradation pathways of bacterial taxa that

were present in contaminated Gulf of Mexico water with the demonstrated uptake of

specific oil constituents. These data revealed a greater microbial capacity for

hydrocarbon degradation than was previously known (Dombrowski et al., 2016).

Studies showed that bioremediation products might be effective in the laboratory but

significantly less so in the field (Mearns, 1997; Venosa et al., 1996; Lee et al., 1997).

This is because laboratory studies cannot always simulate complicated real-world

conditions including factors such as as spatial heterogeneity, biological interactions,

climatic effects, and nutrient mass transport limitations. For example, an

engineered Pseudomonas sp. is capable of degrading camphor, octane, salicylate, and

naphthalene. When such bacteria are introduced into the environment, they disappear

quickly. Their introduction into already colonized niches is very difficult, as most fall

prey to protozoa (Cases and de Lorenzo, 2005). Therefore, field studies and

applications are the ultimate tests or the most convincing demonstration of the

effectiveness of bioremediation products. Compared to microbial products, very few

nutrient additives have been developed and marketed specifically as commercial

bioremediation agents for oil spill cleanup. This is probably because common

fertilizers are inexpensive, readily available, and have been shown to be effective if

used properly (Das & Chandran, 2011). However, due to the limitations of common

fertilizers (e.g., being rapidly washed out due to tide and wave action), several organic

nutrient products, such as oleophilic nutrient products, have recently been evaluated

and marketed as bioremediation agents. These nutrient products were the most well-

known bioremediation agents for oil spill cleanup due to its use on the EVOS in

Prince William Sound, Alaska (Ladousse & Tramier, 1999).

28

CONCLUSIONS

There is no single remediation practice that can achieve 100% removal of oil, and as

such, patches of highly weathered oil can easily remain in marine environments. It is

also impossible to genetically engineer a superbug that can degrade all environmental

oil contamination. However, comparison of the EVOS and the DWH well blowout

results in important similarities and differences that can inform future approaches to

oil spill response. The oil from the DWH spill biodegraded more quickly than oils

from EVOS because it was a 1) light crude oil, 2) highly dispersed in the water

column, 3) subjected to more extensive photodegradation processes, 4) exposed to

warmer water temperatures, 5) present in an offshore location and, 6) microbial

populations were well adapted to hydrocarbon exposure in the Gulf of Mexico

compared to Prince William Sound, AK. In the case of the DWH spill, two weeks

after the accident, no surface oil slick was observed, and concentrations of detectable

oil in the water column were greatly diminished (Operational Science Advisory Team,

2010). Whereas, the EVOS oil required a significantly longer time to biodegrade.

Decisions on remediation strategies such as whether to physically collect the spilled

oil and/or to apply bioremediation approaches should be driven by research and

assessment of both the spill situation and ecosystem conditions, not just the presence

of detectable hydrocarbons. Biostimulation through fertilizer addition was shown to

be effective for the EVOS and increased rates of oil biodegradation; however, the use

of dispersants to accelerate oil biodegradation for the DWH spill was chosen instead

of biostimulation because the DWH spill was located in open ocean, and it is very

expensive and difficult to keep the nutrient levels sufficient to accelerate the speed of

biodegradation. In addition, the advanced molecular techniques for modified

microbial communities were not available at the time of the EVOS. Recently,

considerable progress has been made in evaluating specific strains of bacteria to

degrade one or several compounds of crude oil. The next step is to actually use all this

information to enhance and control the degradability of spilled oil by

bioaugumentation (Brooijmans et al., 2009). With the advancement in microbiology

and molecular engineering technology, we can predict that extensive molecular

analyses of microbial communities will be developed as a result of research from the

DWH, and applied to future oil spills. While scientists are working hard to find

approaches that accelerate the biodegradation rate to remediate oil spill sites via

29

bacteria, the best method is to take care of the ecosystem and minimize the

disturbances to the environment in the first place with preventive measures (i.e.,

avoiding spills).

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